I wonder if the global ear can 'hear' climate change

It seems to me like somebody will try to have it listen, since there are many claims of “climate change” being ubiquitous.

The Global Ear hears all: on February 15, 2013, the CTBTO’s infrasound monitoring stations detected signals made by a meteor that had entered the atmosphere and disintegrated in the skies over Chelyabinsk, Russia. The CTBTO network — the only global one of its kind to detect infrasound — recorded the shock wave caused by the exploding fireball. That data helped scientists to locate the meteor, measure the energy release, its altitude and size.

The CTBTO has the only global network tracking radioactivity and sound waves

From the COMPREHENSIVE NUCLEAR-TEST-BAN TREATY ORGANIZATION

From earthquakes in Nepal to volcanic eruptions in Chile, from meteors crashing to Earth to the songs of migrating whales in the Indian Ocean, The Global Ear hears all.

This universal system of looking, listening and sniffing the Earth is the work of an international organization, the Comprehensive Nuclear-Test-Ban Treaty Organization or CTBTO.

The CTBTO designed and began installing its monitoring network 18 years ago to detect nuclear explosions above ground and underneath. The network is a way to guard against test ban treaty violations. The Comprehensive Nuclear-Test-Ban Treaty (CTBT) bans nuclear explosions by everyone, everywhere — in the atmosphere, underwater and underground.

The network has demonstrated it can do what it was designed to do — to detect nuclear tests with great reliability. For example, on February 12, 2013, 94 of the network’s seismic monitoring stations and two of its infrasound stations detected and alerted member states to a nuclear detonation more than an hour before North Korea announced it had conducted a test.

‘The CTBTO’s International Monitoring System has found a wider mission than its creators ever foresaw: monitoring an active and evolving Earth,’ says Lassina Zerbo, Ph.D., executive secretary of CTBTO. ‘Some compare the system to a combined giant Earth stethoscope and sniffer that looks, listens, feels and sniffs for planetary irregularities.

For example, on February 15, 2013, the CTBTO’s infrasound monitoring stations detected signals made by a meteor that had entered the atmosphere and disintegrated in the skies over Chelyabinsk, Russia. The CTBTO network — the only global one of its kind to detect infrasound — recorded the shock wave caused by the exploding fireball. That data helped scientists to locate the meteor, measure the energy release, its altitude and size.

Another example: the system’s atmospheric sampling tracked the invisible plume of radioactivity from the March 2011 Fukushima Daiichi nuclear power plant disaster, as it spread around the globe. It showed that radioactivity outside of Japan was below harmful levels. That knowledge helped public safety officials around the world understand what course of action to take.

‘It is the only global network which detects atmospheric radioactivity and sound waves which humans cannot hear,’ explains Zerbo.

Scientists, governments, non-governmental organizations and universities have discovered that the massive amounts of data collected by the network have a myriad of uses and benefits.

Other useful spinoffs:

Helping tsunami warning centres issue rapid warnings after a severe earthquake, in near real time

Improving meteorological models for more accurate weather forecasting

Giving an insight into volcanic eruptions

Enhancing the alerts that civil aviation authorities use to warn pilots about damaging volcanic dust in real time

Providing more precise information about climate change

Monitoring drifting icebergs in shipping lanes

Increasing understanding of the structure of the Earth’s inner core

Following the migratory habits and the effects of climate change on marine life

Tracking large storms

To access the data, the CTBTO has created a Virtual Data Exploitation Centre. It provides scientists and researchers from many different disciplines with data for research and enables them to publish new findings: http://www.ctbto.org/specials/vdec

Every two years the CTBTO hosts a scientific and technical conference in Vienna. This year some 1,000 scientists and researchers will gather to share their experience and knowledge and to learn from each other how to use the data. This year’s CTBT Science and Technology conference will be held from June 22-26 at the Hofburg Palace, Vienna, Austria.

Besides the CTBT Science and Technology Conferences, the CTBTO and others support workshops and technical meetings where scientists have the opportunity to meet and exchange knowledge and information.

An extensive monitoring network

The CTBTO’s global monitoring network now comprises 300 stations, some in the most remote and inaccessible areas of the Earth and sea. The network captures four types of data: seismic, hydroacoustic, infrasound and radionuclide. It is about 90 percent complete. When finished, the system will have 337 stations placed globally to monitor every corner of the planet effectively.

Currently, the network collects some 15 gigabytes of data daily, which it sends in real-time to the CTBTO’s data analysis centre in Vienna, Austria. From there, a daily analysis report is sent to the CTBTO’s 183 Member States for their own use and analysis.

‘The International Monitoring System is a fantastic tool for monitoring the planet’s core, atmosphere, oceans, or environment,’ explains Raymond Jeanloz, Ph.D., professor of geophysics and astronomy at the University of California, Berkeley.

‘The CTBTO data give us a glimpse of the Earth’s deep interior -what’s happening there and how it evolved over Earth’s history,’ says Professor Miaki Ishii,Ph.D., Department of Earth and Planetary Sciences, Harvard University.

‘The global data are extremely valuable because they span decades, are high quality and highly calibrated,’ says Randy Bell, director of the CTBTO’s International Data Centre. ‘The data can be used to analyse local, regional or global events.’

Bell says that his primary job is to look for nuclear tests, but allowing the data to be used for science gets more experts looking at the data. ‘What may be noise to me might be a signal to someone else,’ he says.

A wealth of scientific insights

Scientists now mining the trove of CTBTO data accumulated over the past 18 years are gaining new insights into everything from the interior structure of the Earth to learning about atmospheric disturbances and the role they play in changing weather patterns.

For example, the number of seismic events recorded and analysed at the CTBTO’s International Data Centre varies depending on the amount of activity around the world. On a typical day, the centre analyses over 30,000 seismic signals to identify about 130 seismic events that meet stringent criteria. Some events are measured at only a few stations while other events are detected around the globe. Seismic and acoustic waves travel at different speeds and along different paths so analysing the various signals helps pinpoint the time, location and intensity of the recorded events.

‘Beyond nuclear monitoring, we need to understand all kinds of seismic events, which pays off in improving earthquake, fault and tectonic monitoring,’ says Bell. ‘It also has improved our understanding of the Earth itself.’

Though many countries have their own seismic monitoring systems, the CTBTO’s monitors are global, permanent, calibrated and the data are shared equally.

‘One of the key merits of the CTBTO system is that it has a set of fixed stations which provide a stable monitoring baseline,’ says Paul Richards, Ph.D., a seismologist at Columbia University. ‘That stability is useful.’

‘For Sub-Saharan Africa, the CTBTO’s seismic network is instrumental for monitoring and providing data about seismicity in the region,’ says Gerhard Graham, Ph.D., former chief operating officer of the Council for Geoscience, South Africa, and the current Coordinator of the CTBTO’s International Data Centre.

‘The waveform data are used to augment bulletins in Eastern and Southern Africa. The data greatly enhance the accuracy to locate earthquakes in the region. In 2006 in Mozambique, for example, CTBTO data were used to accurately pinpoint the epicentre of a 7.0 magnitude quake. That’s important information to help us understand seismic hazards and to know how best to design and build future sensitive structures such as schools and hospitals,’ says Graham.

The role of infrasound

The CTBTO monitors infrasound – sound waves at frequencies too low to be detected by the human ear — with 48 stations. Four more are under construction and another eight are planned.

Twenty of the CTBTO’s infrasound monitoring stations detected signals made by a meteor that had entered the atmosphere and disintegrated in the skies over Chelyabinsk, Russia on February 15, 2013.

A station in Antarctica, some 15,000 kilometres away, detected the meteor’s sub-audible sound. The station detected sound waves generated by the blast twice, travelling in opposite directions, as they circumnavigated the Earth. A station in Alaska, some 6,500 kilometres away, clocked it circling the Earth three times.

Fifteen stations recorded the meteor that exploded over Sulawesi, Indonesia, in October 2009. The Chelyabinsk meteor was ten to fifty times more energetic.

The sensitivity of the CTBTO’s infrasound sensors helps scientist to gauge the number of meteorites burning in the atmosphere; many of these airbursts would otherwise go unnoticed.

Correlating infrasound and other observations of meteors is giving scientists a better understanding of the populations of Near Earth Objects and insights into the process that leads to the formation of the solar system.

The ability of the system to track atmospheric disturbances, whether volcanic eruptions, severe storms or other large scale turbulence, provides a way to improve weather forecasts and, by using nearly two decades of accumulated data, track climate change.

Elisabeth Blanc, Ph.D., Research Director at France’s Atomic Energy and Alternative Energies Commission, heads a European project to improve long-term weather forecasting models based on temperature and wind changes in the stratosphere, using some of the CTBTO’s infrasound data.

‘Two weeks after major stratospheric warming was detected at the end of 2012, the weather in Europe changed dramatically,’ says Blanc. ‘We think this was related to stratospheric warming.

‘If our research confirms the effects of these kinds of changes, weather models could forecast ahead by several weeks or even a season. That would be very important, but we are not there yet.’

Listening underwater

With its continuous monitoring of underwater sounds, the CTBTO’s network of 11 underwater listening posts adds another dimension to the network. Located deep in some of the world’s most remote waters, these hydroacoustic stations listen to earthquakes in the Andes Mountains and around the northern Pacific. The data from the CTBTO’s hydroacoustic as well as seismic stations are used for tsunami warnings.

The data are provided in near real-time to tsunami warning centres, in particular those covering the Pacific and Indian Oceans, to help them issue more timely and precise warnings. At present, tsunami warning centres in 13 countries with a high tsunami risk receive data from around 100 CTBTO stations.

These stations also detect and track chunks of breaking icebergs and the migration of whales.

‘The data are a treasure trove for those studying marine mammals,’ says Mark Prior, Ph.D., a former CTBTO staff member now with the Netherlands Organization for Applied Scientific Research. ‘The main thing limiting use of the data is our imagination,’ he says.

Some researchers are using the data to track the migratory habits of a particular species of Blue Whale that resides in the Indian Ocean but is also seen in Alaska. Such studies help researchers estimate the densities and size of the whale population.

The system could also help determine the time and location of large aircraft impacts and explosions. In the case of Malaysia Airlines flight MH370, which is believed to have crashed into the ocean, Australian and U.S. researchers are still examining the data for clues of the airliner’s fate.

Detecting atmospheric radioactivity

Every day, the International Data Centre analyses over a thousand atmospheric radiation spectra from around the globe to detect minute traces of rare isotopes that might indicate nuclear activity. The ability to track radioactive particles and noble gases, especially xenon, a gas emitted in nuclear explosions, adds another dimension to the network. Forty of the 80 radioactive nuclide detecting stations will be equipped to detect noble gases, including xenon, which are difficult to contain underground after a below-the-surface nuclear test. These gases are not washed out of the atmosphere by precipitation.

‘CTBTO monitoring has detected surprising amounts of xenon,’ explains Gerhard Wotawa, Ph.D., a senior meteorologist with the Central Institute for Meteorology and Geodynamics in Austria. ‘The source is not nuclear power plants or nuclear tests as first suspected, but the production of medical radioisotopes, a discovery that has prompted a search for ways to limit the emissions and reduce the global levels of radioactivity. Only a few facilities manufacture these isotopes, but stopping them is not an option. If we stop production, we would run out of cancer treatments,’ he says.

Since the issue came to light, the CTBTO has joined forces with 10 medical isotope production companies, which have vowed to reduce emissions or bring xenon emissions to zero.

The CTBTO also tracks radioactivity which comes from the plume of active volcanoes and beryllium-7 particles which are produced naturally and move with atmospheric circulations from the stratosphere seasonally to ground level. Observing large-scale atmospheric circulation patterns is useful for understanding weather patterns like tropical storms.

Maintaining the CTBTO system

‘The nations of the world have invested about U.S. $1 billion to create The Global Ear,’ says Zerbo. ‘Every year they continue their investment, hoping it will never have to be used for its intended purpose of detecting a violation of the Nuclear-Test-Ban Treaty. Civil and scientific spinoffs show the world immediate payback and in turn increase support for the Treaty.

‘As more scientists and organizations make use of the data, the value has become ever more apparent,’ says Zerbo.

Have no fear, the “boomers” have been collecting data for decades.
What else have they to do ?.
You would have to be insane to imagine you could win a war against a foe, that can nuke your command and control sites from under the ocean.
So, you wanna play ?

During the 15% of the year that Germany’s 25,000 turbines might be turning, maybe CTBTO could detect their infrasound. Perhaps they could issue early alerts for bird butchering along major global flyways …

Sound propagation in the sea is affected by physical attributes of temperature and thermal stratification. Sound propagation is also affected by biological attributes such as vertical migration of plankton as deep scattering layers. Have the alleged sequestered heat or other global warming effects changed sound propagation?

Has been for quite some time. That’s why instruments based on Nuclear Magnetic Resonance Imaging (NMRI) became shortened to Magnetic Resonance Imaging (MRI) for public consumption in the medical arena.

I don’t even need a thermometer to tell me that it isn’t warming – we had to abandon sitting out in the garden this afternoon, in the middle of England in the middle of June. Same as always, please fetch me a cardi.

“It showed that radioactivity outside of Japan was below harmful levels. That knowledge helped public safety officials around the world understand what course of action to take.”
My thought would be, “no action at all”. Of course that would not appropriatly justify their existance.

‘Every year they continue their investment, hoping it will never have to be used for its intended purpose of detecting a violation of the Nuclear-Test-Ban Treaty.
According to the article, didn’t this happen already–North Korea?

Climate change is like pornography, you know it when you see it, or hear it, or whatever.
Actually the data is interesting, and seems it has a number of productive uses. However they look like pandering idiots when they say this.
“Following the migratory habits and the effects of climate change on marine life”
When what they can only possibly provide is this
“Follow the migratory habits of marine life”
After following the migratory habits of marine life it may be possible to tie it to changes in climate or perhaps any combination of a dozen other factors. What you don’t do is assume marine life is migrating due to AGW and then conclude all of your results are explained by AGW. Replace AGW with God, aliens, or ESP and that kind of argument magically always seems to work in your favor.
It is remarkable in a time of tremendous technological advancement across diverse practical application, climate science insists on forcing this age to be known as the age when “Science went Stupid”.

At mean sea level, the average temperature is 288.2 K, corresponding to a mean adiabatic sound speed (c) of 340.4 m/s (c2 = 401.875 m2 s−2 K−1T, where T is the temperature in degrees K. This is a very good approximation below 95 km.). As altitude increases and the atmospheric mass density decreases, the temperature decreases with an average adiabatic lapse rate of approximately 6 K/km. Increased absorption of solar UV radiation, itself a product of UV absorption, causes the temperature gradient to change sign above the tropopause. The stratopause temperature maximum occurs roughly at the altitude of maximum absorption; about 270 K at 50 km corresponding to an average adiabatic sound speed of 329.4 m/s.

A large meteor entered the atmosphere above northeastern Oregon on 19 February 2008 at 530 PST. Several hundreds of broadband seismic stations in the U.S. Pacific Northwest recorded acoustic-to-seismic coupled signals from this event

The average lapse rate of 6 K km−1 corresponds to a decrease in sound speed of nearly 4ms−1 per kilometer of altitude through the relation c = 20.05T1/2 ms−1, where T is the temperature in degrees Kelvin (K). The typical decrease in sound speed with altitude causes infrasound to refract upward away from Earth’s surface. However, cooling air temperatures near ground level at night and early in the day can combine with the tropospheric jet stream to give rise to short-lived tropospheric ducts

. . .The arrays in this global network consist of array elements, based on microbarometers, that are capable of measuring infrasound in the range of at least 0.02 to 4 Hz with amplitudes of mPa up to tens of pascals.. . .microbaroms typically occur around 0.2 Hz.
. . .Infrasound propagation is mainly controlled by the effective sound speed, i.e., the propagation velocity as function of the temperature and wind along the source-receiver trajectory. At long ranges, say 200 km and more, there are two regions in the atmosphere which lead to the refraction of waves due to an increase in effective velocity. If the gradient in the effective sound profile is strong enough, waves are refracted back to the earth’s surface. This is the case in the stratosphere around 50 km altitude and the thermosphere from 100 km and upwards.

The ‘Global Ear’ inspires thoughts of what bears do in the woods, and whether it makes a sound.
Can you hear me now?
“How loud, brown cow?”
(my apologies, I find myself vulnerable to silliness at times)

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